<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">386403333</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180307112209.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">161130e198907  xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1017/S0016756800006531</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">S0016756800006531</subfield>
   <subfield code="2">pii</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)cambridge-10.1017/S0016756800006531</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="3">
   <subfield code="a">An application of cathodoluminescence microscopy to the study of textures and reactions in high-grade marbles from Connemara, Ireland</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Upper amphibolite facies dolomite and calcite marbles from the Dalradian Connemara Marble Formation of western Ireland display a wide range of textures when viewed in cathodoluminescence that are invisible in transmitted light. Examples observed include growth zones in calcite that appear to represent the infilling of a metamorphic secondary porosity, produced by the large reduction in solid volume accompanying growth of tremolite from dolomite and quartz. Retrograde phenomena are widespread, and include both carbonate pseudomorphs after tremolite and coarse veining, which is in optical continuity with peak metamorphic calcite but otherwise indistinguishable from it. Admixture of such widely differing calcite types may account for scatter in some stable isotope studies of marbles.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Copyright © Cambridge University Press 1989</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Yardley</subfield>
   <subfield code="D">B. W. D.</subfield>
   <subfield code="u">Department of Earth Sciences, University of Leeds, Leeds LS2 9JT, U.K.</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Lloyd</subfield>
   <subfield code="D">G. E.</subfield>
   <subfield code="u">Department of Earth Sciences, University of Leeds, Leeds LS2 9JT, U.K.</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Geological Magazine</subfield>
   <subfield code="d">Cambridge University Press</subfield>
   <subfield code="g">126/4(1989-07), 333-337</subfield>
   <subfield code="x">0016-7568</subfield>
   <subfield code="q">126:4&lt;333</subfield>
   <subfield code="1">1989</subfield>
   <subfield code="2">126</subfield>
   <subfield code="o">GEO</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1017/S0016756800006531</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1017/S0016756800006531</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Yardley</subfield>
   <subfield code="D">B. W. D.</subfield>
   <subfield code="u">Department of Earth Sciences, University of Leeds, Leeds LS2 9JT, U.K</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Lloyd</subfield>
   <subfield code="D">G. E.</subfield>
   <subfield code="u">Department of Earth Sciences, University of Leeds, Leeds LS2 9JT, U.K</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Geological Magazine</subfield>
   <subfield code="d">Cambridge University Press</subfield>
   <subfield code="g">126/4(1989-07), 333-337</subfield>
   <subfield code="x">0016-7568</subfield>
   <subfield code="q">126:4&lt;333</subfield>
   <subfield code="1">1989</subfield>
   <subfield code="2">126</subfield>
   <subfield code="o">GEO</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="b">CC0</subfield>
   <subfield code="u">http://creativecommons.org/publicdomain/zero/1.0</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-cambridge</subfield>
  </datafield>
 </record>
</collection>
